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Biomaterials.. Interfacial Phenomena and Applications - download pdf or read online

By S.L.& Peppas, N.A.(eds.) Cooper

ISBN-10: 0841206317

ISBN-13: 9780841206311

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Detwiler, A. 1989. Comments on "Homogeneous nucleation rate for highly supercooled cirrus cloud droplets. J. Atmos. Sci. 46, 2344-2345. Dowling, D. , and Radke, L. F. 1990. A summary of the physical properties of cirrus clouds. J. Appl. Meteor. 29, 970-978. 52 Flatau, P. , Stephens, G. , and Draine, B. T. 1988. Scattering on hexagonal ice crystals: discrete dipole and anomalous diffraction approximations. 72-75. , and Liou, K N. 1993. Parameterization of the radiative properties of cirrus clouds.

Dry air produced in this manner is distributed throughout the midlatitudes in the form of filaments. General circulation models which fail to resolve these filaments would mix the dry air into adjoining moist air, spuriously lowering the relative humidity of the moist filaments and thus inhibiting condensation. The extra tropical mixing zone is bounded by a subtropical barrier, across which mixing is much weaker. Nonetheless, vigorous recirculating eddies of the subtropical "surf zone" episodically inject dry subtropical air and dry air of high-altitude midlatitude provenance into the tropics.

INTRODUCTION Cirrus clouds are rapidly gaining increased attention as an important component of the climate system. There are some solid physical reasons for that: cirrus are extensive in space and time. In addition, they are cold enough to cause a strong greenhouse effect. However, the problem of quantifying their influence on the present climate has remained essentially unresolved and we are even farther from being able to predict their response to a changing climate. While the issue of understanding cloud feedback mechanisms is not limited to cirrus these clouds have some characteristics which complicate the problem.

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Biomaterials.. Interfacial Phenomena and Applications by S.L.& Peppas, N.A.(eds.) Cooper

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